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== Weather and climate == | == Weather and climate == | ||
[[File:Qu_Coreolis_Atmosphere.png|500px|thumb|right|Fig. 5. The Coriolis forces on rising and falling air masses create horizontal vortices.]]Due to the rotation of the tubes, there are strong horizontal Coriolis forces whose effects can be seen | [[File:Qu_Coreolis_Atmosphere.png|500px|thumb|right|Fig. 5. The Coriolis forces on rising and falling air masses create horizontal vortices.]]Due to the rotation of the tubes, there are strong horizontal Coriolis forces whose effects can be seen when observing weather patterns and when any object falls from a great height. Falling objects, including rain and cold masses of air, lack the rotational velocity of parts of the tube further from the centre. From the perspective of someone standing within the tube, falling objects appear to be drawn backwards relative to this movement as they fall. This backwards direction is called ''vo'' in Iliaqu and can be translated as 'south' as it is 90° to the right of the direction of dawn light. | ||
Rising masses of warm air retain the momentum they received from the rotation of the outer parts of the tube as they enter higher (more inner) parts of the tube, causing their apparent path to curve 'forwards'. This forward direction is called ''guo'' in Iliaqu and can be translated as 'north' as it is 90° to the left of the dawn light. | Rising masses of warm air retain the momentum they received from the rotation of the outer parts of the tube as they enter higher (more inner) parts of the tube, causing their apparent path to curve 'forwards'. This forward direction is called ''guo'' in Iliaqu and can be translated as 'north' as it is 90° to the left of the dawn light. |
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